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Predictive Mineralogy

Possible unrecorded species at Sæteråsen Niobium-deposit, Hedrum, Larvik, Vestfold, Norway

This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.

Possible missing speciesFormulaMatch %Due to recorded presence of
CalciteCaCO398.55%Andradite (61.21 %), Clinozoisite (56.64 %), Phlogopite (55.90 %), Titanite (52.17 %), Zirkelite (59.38 %)
PyriteFeS288.72%Clinozoisite (51.74 %), Hematite (50.17 %), Zirkelite (53.13 %)
Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)78.92%Clinozoisite (56.31 %), Zoisite (51.75 %)
PyrrhotiteFe1-xS62.50%Zirkelite (62.50 %)
DolomiteCaMg(CO3)259.37%Zirkelite (59.38 %)
BaddeleyiteZrO253.12%Zirkelite (53.13 %)
DiopsideCaMgSi2O653.12%Zirkelite (53.13 %)
MuscoviteKAl2(AlSi3O10)(OH)252.79%Albite (52.80 %)
NephelineNa3K(Al4Si4O16)50.71%Aegirine-augite (50.72 %)
IlmeniteFe2+TiO350.00%Zirkelite (50.00 %)
RutileTiO250.00%Zirkelite (50.00 %)

Key: Mineral matches key element mineralogy of deposit Key element(s) in mineral not listed for deposit (-20% score)


Predicting paragenetic modes of deposit

Green indicates almost certain match based on minerals unique to a certain deposit type. Yellow indicates a possibly poor match, but should not be entirely discounted. Scores > 100 indicate strong confidence.

Paragenetic ModeScore
34 : Complex granite pegmatites50
35 : Ultra-alkali and agpaitic igneous rocks27
26 : Hadean detrital minerals26
36 : Carbonatites, kimberlites, and related igneous rocks9
3 : Solar nebular condensates (CAIs, AOAs, URIs)7
37 : Layered igneous intrusions and related PGE minerals7
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)5
31 : Thermally altered carbonate, phosphate, and iron formations5
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)3
43 : Shear-induced minerals (including mylonite/slickensides)2